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四川双河岩盐矿区钻探、物探综合研究
引用本文:寸树苍,石应骏,陈华玢.四川双河岩盐矿区钻探、物探综合研究[J].成都理工大学学报(自然科学版),1996(1).
作者姓名:寸树苍  石应骏  陈华玢
作者单位:成都理工学院信息工程与地球物理系
摘    要:双河岩盐矿区的钻探工程发现,该区岩盐层厚度变化急剧,并且埋藏浅者厚度大,表明有沉积期后改造过程,或称“盐运动构造”。经大地电磁测深和高精度重力测量,进一步发现在岩盐层上方和下方各有一个“泥辟构造”存在。重力异常还显示出岩盐层厚度向两侧根快变薄、尖灭的特点。文章综合钻探、物探研究成果,对岩盐层富集区进行了圈定。

关 键 词:大地电磁测深  盐运动构造  泥辟构造

A SYNTHESIS STUDY OF DRILL AND GEOPHYSICAL OPERATIONS FOR THE SHUANGHE ROCK SALT MINING AREA
Cun Shucang,Shi Yingjun,Chen Huafen.A SYNTHESIS STUDY OF DRILL AND GEOPHYSICAL OPERATIONS FOR THE SHUANGHE ROCK SALT MINING AREA[J].Journal of Chengdu University of Technology: Sci & Technol Ed,1996(1).
Authors:Cun Shucang  Shi Yingjun  Chen Huafen
Abstract:The drill operation has found that the thickness of the rock salt layer varies greatlyand that the shallower layer has greater thickness in the Shuanghe rock salt mining area. This indicates that there is a reworking process after deposition,or "salt moving structure". The data ofmagnetotelluric sounding and high resolution gravity survey reveal that there is a "mud diapirismstructure" on and beneath the rock salt layer.The gravity anomalies also reveal the feature thatthe thickness of the layer becomes thin and wedging out along its sides. Having synthesized theresults of drill and geophysicai operations,the authors outlined the areas rich in rock salt layers.
Keywords:magnetotelluric sounding  salt moving structure  mud diapirism structure  
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